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An arbitrary Lagrangian-Eulerian σ (ALES) model with non- hydrostatic pressure for shallow water flows

机译:具有非静水压力的浅水流动的任意Lagrangian-Eulerianσ(ALES)模型

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An arbitrary Lagrallgian-Eulerian model in the a coordinate system (ALES) is developcd for shallow water flows, based on the unsteady Reynolds-averaged Navier Stokes equations. Unlike the conventional a coordinate system. non-hydrostatic pressure is in- corporated and the effect of a moving fl-e e-surface included giving a general scheme. The standard k-ε turbulence model is used to calculate the eddy viscosity. Wave flows over bars are appropriate test cases for which experimental data are available and comparisons are favourab1e. The model is also applied to the important practical problem of wave and wave/current flows over a trench, for which experimental data are available only for the steady current alone case. The inclusion of vertical grid velocity has negligible effect on computational efficiency. The solution of Poisson's equation for non-hydrostatic pressure at each time step is solved efficiently by the conjugate gradient method but represents the main component of computer time. The model may readily be extended to three di- mensions.
机译:基于非稳态的雷诺平均Navier Stokes方程,开发了浅水流动的坐标系(ALES)中的任意Lagrallgian-Eulerian模型。与常规坐标系统不同。将非静水压力纳入其中,并包括移动的fl e表面的影响,从而提供了一个一般方案。使用标准的k-ε湍流模型来计算涡流粘度。棒上的波浪流动是合适的测试用例,可提供实验数据并进行比较。该模型还适用于重要的实际问题,即波和在沟槽上流动的波/电流,仅对于稳定电流情况,实验数据才可用。包括垂直网格速度对计算效率的影响可以忽略不计。共轭梯度法可以有效地求解每个时间步的非静水压力的泊松方程解,但它代表了计算机时间的主要组成部分。该模型可以很容易地扩展到三个维度。

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